Слайд 2Performed:
Tumanova Anastasia
Слайд 3The Australian continent is located within the three main warm climatic zones
of the southern hemisphere:subequatorial, tropical , subtropical.
Слайд 4Subequatorial climate characteristic for Northern and the North-Eastern part of the Australian
continent .It differs by stream of temperatures and high precipitation . Wet North-West monsoon brings rainfall here and rainfall is usually in summer. In winter, in the dry period of the year, it rains occasionally.
Слайд 5Tropical belt of the Australian continent is formed by two main types
of climate:tropical wet, tropical dry.
Слайд 6A tropical monsoon climate is inherent in the far Eastern part of
Australia, which is in the zone of action of the South-Eastern winds.
Слайд 7These winds bring with them to the mainland air masses from the
Pacific ocean.
Слайд 8Australia is the driest сontinent of the Earth, and one of the
most characteristic features of the nature of it is a wide spread of desert.
Слайд 9The Central and Western part of Australia, earn about 250-300 mm of
precipitation per year, but these are minor precipitation is irregular, in general there are no rains, and sometimes , for two or three days, and then for a few hours falls all of the annual precipitation.
Слайд 11Within the subtropical belt Australia there are three types of climate: Mediterranean,
subtropical continental and subtropical moist.
Слайд 12The Mediterranean climate is typical for the South-Western part of Australia. The
climate of this part of the country is similar to the climate of the European Mediterranean countries- Spain and southern France.
Слайд 13The zone of subtropical continental climate covers the South part of the
continent. The main features of the climate are small quantity of precipitation and relatively large annual variation in temperature.
Слайд 14Hot climate and low and irregular precipitation in most part of the
continent leads to he fact that almost 60% of its territory are deprived of runoff to the ocean.